Nd isotopes of ODP Sites 146-893 and 167-1017 samples
Changes in the source of intermediate waters to the southern California margin may have caused variations in seafloor oxygen levels on stadial–interstadial time scales. We test this hypothesis using the Nd isotopic composition of benthic foraminifera and fossil fish debris from ODP Sites 893 and 101...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2013
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.816402 https://doi.org/10.1594/PANGAEA.816402 |